The possible impact of gas-bearing fluids on sediment in the arch Fedynskogo (Barents sea)

A comparative analysis of facies and composition of precipitation on the bottom areas where the discharge of methane fluid occurs rapidly or not registered. Effect of gaseous fluids on postsedimentary transformation of clay minerals not found. Possible local manifestation of the fluid can be lithoge...

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Bibliographic Details
Main Authors: N P Chamov, V V Kostyleva, S Yu Sokolov, A E Kotelnikov
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Peoples’ Friendship University of Russia (RUDN University) 2015
Subjects:
подводная мерзлота
метаноносные флюиды
флюидный литогенез
Engineering (General). Civil engineering (General)
TA1-2040
Barents Sea
The Arch
Online Access:https://doaj.org/article/b4fbef5de6e24933a9eaf602a3629a05
Description
Summary:A comparative analysis of facies and composition of precipitation on the bottom areas where the discharge of methane fluid occurs rapidly or not registered. Effect of gaseous fluids on postsedimentary transformation of clay minerals not found. Possible local manifestation of the fluid can be lithogenesis authigenic carbonate formation.

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